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Parallel Regions Soil Model in MALZ

The Parallel Regions soil model, where the effects of Boundaries between Regions are explicitly modelled using currents on the discretized boundaries, is still relatively recent: it was introduced in V18.0 and it featured an improved tiling algorithm and a new UI in V19.0. Users could then graphically specify a point on one boundary and the thicknesses of regions between parallel boundaries to define the model.

Example Image
User Interface for the Parallel Regions soil model in Soil Model Editor.

Next we discuss its usage: when results will be the same as those of the Multi-Region soil model, where conductors are assigned to soil regions as chosen by the user and which uses an approximation where boundaries are ignored, and when they could be different.

Example Image
Touch voltage on a well-coated pipeline in a typical Right-of-Way situation,
for the Multi-Region (User Assigned) and the Parallel Regions soil models.

As the image above illustrates with a touch voltage plot on a pipeline, for standard right-of-way situations where the pipeline is well coated, the two models give the same results and there is no need for using the Parallel Regions soil model, which is more computationally demanding.

In other situations, the effects of boundaries may be very important. It is relevant to consider the pedagogical details in the case of a long bare conductor that straddles three soil regions, each being a different multi-layer horizontal soil. This case is a situation where different soil models give very different results since the leakage current of the conductor is very sensitive to the local soil.

This different behavior is illustrated here for three soil models: one three-region Parallel Regions soil model, the Multi-Region model obtained by ignoring the boundaries, and the Vertical soil model obtained by using the bottom layer resistivity of each multi-layer horizontal soil model of the Parallel Regions model.

Example Image
Scalar potential following a long bare conductor energized at one end.

After building the models, the strategies for validating the results include using a simpler and computationally faster uniform soil model to calibrate the discretization of the boundaries and visualizing the discretization pattern and the currents on the boundaries.

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